Frost Thawing

Frost thawing refers to the process where water in soil or rock freezes when temperatures drop, then thaws as temperatures rise. When water freezes, it expands, which can create pressure in cracks and openings. This cycle of freezing and thawing can lead to the gradual breaking apart of materials, such as rocks and concrete. Over time, this natural process can cause significant erosion and damage to structures, roads, and landscapes. It’s a common occurrence in climates with fluctuating temperatures, and understanding it is crucial for construction and environmental management.